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class="vector-toc-text"> 1.5 Groundwater extraction </div> </a> <ul id="toc-Groundwater_extraction-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Geothermal_energy" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Geothermal_energy"> <div class="vector-toc-text"> 1.6 Geothermal energy </div> </a> <ul id="toc-Geothermal_energy-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Hydraulic_fracturing" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Hydraulic_fracturing"> <div class="vector-toc-text"> 1.7 Hydraulic fracturing </div> </a> <ul id="toc-Hydraulic_fracturing-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Carbon_capture_and_storage" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Carbon_capture_and_storage"> <div class="vector-toc-text"> 1.8 Carbon capture and storage </div> </a> <ul id="toc-Carbon_capture_and_storage-sublist" class="vector-toc-list"> <li id="toc-Risk_analysis" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Risk_analysis"> <div class="vector-toc-text"> 1.8.1 Risk analysis </div> </a> <ul id="toc-Risk_analysis-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Monitoring" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Monitoring"> <div class="vector-toc-text"> 1.8.2 Monitoring </div> </a> <ul id="toc-Monitoring-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Failure_mechanisms_due_to_fluid_injection" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Failure_mechanisms_due_to_fluid_injection"> <div class="vector-toc-text"> 1.8.3 Failure mechanisms due to fluid injection </div> </a> <ul id="toc-Failure_mechanisms_due_to_fluid_injection-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Comparison_of_risks_due_to_CCS_versus_other_injection_methods" 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vector-toc-toggle"> Toggle Risk analysis subsection </button> <ul id="toc-Risk_analysis_2-sublist" class="vector-toc-list"> <li id="toc-Risk_factors" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Risk_factors"> <div class="vector-toc-text"> 2.1 Risk factors </div> </a> <ul id="toc-Risk_factors-sublist" class="vector-toc-list"> <li id="toc-Ground_shaking" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Ground_shaking"> <div class="vector-toc-text"> 2.1.1 Ground shaking </div> </a> <ul id="toc-Ground_shaking-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Probabilistic_seismic_hazard_analysis" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Probabilistic_seismic_hazard_analysis"> <div class="vector-toc-text"> 2.2 Probabilistic seismic hazard analysis </div> </a> <ul id="toc-Probabilistic_seismic_hazard_analysis-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Calculating_Seismic_Risk" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Calculating_Seismic_Risk"> <div class="vector-toc-text"> 2.3 Calculating Seismic Risk </div> </a> <ul id="toc-Calculating_Seismic_Risk-sublist" class="vector-toc-list"> <li id="toc-Earthquake_source_characterization" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Earthquake_source_characterization"> <div class="vector-toc-text"> 2.3.1 Earthquake source characterization </div> </a> <ul id="toc-Earthquake_source_characterization-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Recurrence_pattern" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Recurrence_pattern"> <div class="vector-toc-text"> 2.3.2 Recurrence pattern </div> </a> <ul id="toc-Recurrence_pattern-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Ground_motions" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Ground_motions"> <div class="vector-toc-text"> 2.3.3 Ground motions </div> </a> <ul id="toc-Ground_motions-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Seismic_hazard" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Seismic_hazard"> <div class="vector-toc-text"> 2.3.4 Seismic hazard </div> </a> <ul id="toc-Seismic_hazard-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Exposure_and_vulnerability" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Exposure_and_vulnerability"> <div class="vector-toc-text"> 2.3.5 Exposure and vulnerability </div> </a> <ul id="toc-Exposure_and_vulnerability-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Seismic_risk" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Seismic_risk"> <div class="vector-toc-text"> 2.3.6 Seismic risk </div> </a> <ul id="toc-Seismic_risk-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Risk_Mitigation" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Risk_Mitigation"> <div class="vector-toc-text"> 2.4 Risk Mitigation </div> </a> <ul id="toc-Risk_Mitigation-sublist" class="vector-toc-list"> <li id="toc-Traffic_Light_System" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Traffic_Light_System"> <div class="vector-toc-text"> 2.4.1 Traffic Light System </div> </a> <ul id="toc-Traffic_Light_System-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> </ul> </li> <li id="toc-Nuclear_explosions" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Nuclear_explosions"> <div class="vector-toc-text"> 3 Nuclear explosions </div> </a> <ul id="toc-Nuclear_explosions-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-U.S._National_Research_Council_report" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#U.S._National_Research_Council_report"> <div class="vector-toc-text"> 4 U.S. National Research Council report </div> </a> <ul id="toc-U.S._National_Research_Council_report-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-List_of_induced_seismic_events" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#List_of_induced_seismic_events"> <div class="vector-toc-text"> 5 List of induced seismic events </div> </a> <button aria-controls="toc-List_of_induced_seismic_events-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> Toggle List of induced seismic events subsection </button> <ul id="toc-List_of_induced_seismic_events-sublist" class="vector-toc-list"> <li id="toc-Table" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Table"> <div class="vector-toc-text"> 5.1 Table </div> </a> <ul id="toc-Table-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-References" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#References"> <div class="vector-toc-text"> 6 References </div> </a> <ul id="toc-References-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Further_reading" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Further_reading"> <div class="vector-toc-text"> 7 Further reading </div> </a> <ul id="toc-Further_reading-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-External_links" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#External_links"> <div class="vector-toc-text"> 8 External links </div> </a> <ul id="toc-External_links-sublist" class="vector-toc-list"> </ul> </li> </ul> </div> </div> </nav> </div> </div> <div class="mw-content-container"> <main id="content" class="mw-body"> <header class="mw-body-header vector-page-titlebar"> <nav aria-label="Contents" class="vector-toc-landmark"> 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Available in 14 languages" > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-14" aria-hidden="true" > 14 languages </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/%C4%B0nduktiv_seysmiklik" title="İnduktiv seysmiklik – Azerbaijani" lang="az" hreflang="az" data-title="İnduktiv seysmiklik" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target">Azərbaycanca</a></li><li class="interlanguage-link interwiki-zh-min-nan mw-list-item"><a href="https://zh-min-nan.wikipedia.org/wiki/%C3%8Dn-i%C3%BA-s%C3%A8ng_t%C4%93-ch%C3%ACn-t%C5%8D%CD%98" title="Ín-iú-sèng tē-chìn-tō͘ – Minnan" lang="nan" hreflang="nan" data-title="Ín-iú-sèng tē-chìn-tō͘" data-language-autonym="閩南語 / Bân-lâm-gú" data-language-local-name="Minnan" class="interlanguage-link-target">閩南語 / Bân-lâm-gú</a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Induzierte_Seismizit%C3%A4t" title="Induzierte Seismizität – German" lang="de" hreflang="de" data-title="Induzierte Seismizität" data-language-autonym="Deutsch" data-language-local-name="German" class="interlanguage-link-target">Deutsch</a></li><li class="interlanguage-link interwiki-el mw-list-item"><a href="https://el.wikipedia.org/wiki/%CE%A0%CF%81%CF%8C%CE%BA%CE%BB%CE%B7%CF%83%CE%B7_%CF%83%CE%B5%CE%B9%CF%83%CE%BC%CF%8E%CE%BD" title="Πρόκληση σεισμών – Greek" lang="el" hreflang="el" data-title="Πρόκληση σεισμών" data-language-autonym="Ελληνικά" data-language-local-name="Greek" class="interlanguage-link-target">Ελληνικά</a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D9%84%D8%B1%D8%B2%D9%87%E2%80%8C%D8%AE%DB%8C%D8%B2%DB%8C_%D8%A7%D9%84%D9%82%D8%A7%DB%8C%DB%8C" title="لرزه‌خیزی القایی – Persian" lang="fa" hreflang="fa" data-title="لرزه‌خیزی القایی" data-language-autonym="فارسی" data-language-local-name="Persian" class="interlanguage-link-target">فارسی</a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/S%C3%A9isme_induit" title="Séisme induit – French" lang="fr" hreflang="fr" data-title="Séisme induit" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target">Français</a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%EC%9D%B8%EA%B3%B5%EC%A7%80%EC%A7%84" title="인공지진 – Korean" lang="ko" hreflang="ko" data-title="인공지진" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target">한국어</a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%A8%D7%A2%D7%99%D7%93%D7%95%D7%AA_%D7%90%D7%93%D7%9E%D7%94_%D7%9E%D7%95%D7%A9%D7%A8%D7%95%D7%AA" title="רעידות אדמה מושרות – Hebrew" lang="he" hreflang="he" data-title="רעידות אדמה מושרות" data-language-autonym="עברית" data-language-local-name="Hebrew" class="interlanguage-link-target">עברית</a></li><li class="interlanguage-link interwiki-kk mw-list-item"><a href="https://kk.wikipedia.org/wiki/%D0%90%D0%BD%D1%82%D1%80%D0%BE%D0%BF%D0%BE%D0%B3%D0%B5%D0%BD%D0%B4%D1%96%D0%BA_%D0%B6%D0%B5%D1%80_%D1%81%D1%96%D0%BB%D0%BA%D1%96%D0%BD%D1%83%D1%96" title="Антропогендік жер сілкінуі – Kazakh" lang="kk" hreflang="kk" data-title="Антропогендік жер сілкінуі" data-language-autonym="Қазақша" data-language-local-name="Kazakh" class="interlanguage-link-target">Қазақша</a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E4%BA%BA%E5%B7%A5%E5%9C%B0%E9%9C%87" title="人工地震 – Japanese" lang="ja" hreflang="ja" data-title="人工地震" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target">日本語</a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Sejsmiczno%C5%9B%C4%87_indukowana" title="Sejsmiczność indukowana – Polish" lang="pl" hreflang="pl" data-title="Sejsmiczność indukowana" data-language-autonym="Polski" data-language-local-name="Polish" class="interlanguage-link-target">Polski</a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%9D%D0%B0%D0%B2%D0%B5%D0%B4%D0%B5%D0%BD%D0%B0_%D1%81%D0%B5%D0%B9%D1%81%D0%BC%D1%96%D1%87%D0%BD%D0%B0_%D0%B0%D0%BA%D1%82%D0%B8%D0%B2%D0%BD%D1%96%D1%81%D1%82%D1%8C" title="Наведена сейсмічна активність – Ukrainian" lang="uk" hreflang="uk" data-title="Наведена сейсмічна активність" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target">Українська</a></li><li class="interlanguage-link interwiki-ur mw-list-item"><a href="https://ur.wikipedia.org/wiki/%D8%A7%D9%86%DA%88%DB%8C%D9%88%DA%88%D8%B3%DA%88_%D8%B3%DB%8C%D8%B3_%D9%85%DB%8C%D9%B9%DB%8C" title="انڈیوڈسڈ سیس میٹی – Urdu" lang="ur" hreflang="ur" data-title="انڈیوڈسڈ سیس میٹی" data-language-autonym="اردو" data-language-local-name="Urdu" class="interlanguage-link-target">اردو</a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E4%BA%BA%E5%B7%A5%E5%9C%B0%E9%9C%87" title="人工地震 – Chinese" lang="zh" hreflang="zh" data-title="人工地震" data-language-autonym="中文" data-language-local-name="Chinese" class="interlanguage-link-target">中文</a></li> </ul> <div class="after-portlet after-portlet-lang"><a href="https://www.wikidata.org/wiki/Special:EntityPage/Q1394636#sitelinks-wikipedia" title="Edit interlanguage links" class="wbc-editpage">Edit links</a></div> </div> </div> </div> </header> <div class="vector-page-toolbar"> <div 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srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/a0/Earthquake_-_The_Noun_Project.svg/120px-Earthquake_-_The_Noun_Project.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/a0/Earthquake_-_The_Noun_Project.svg/160px-Earthquake_-_The_Noun_Project.svg.png 2x" data-file-width="512" data-file-height="410" /></a></td></tr><tr><td class="sidebar-content"> <div class="sidebar-list mw-collapsible mw-collapsed"><div class="sidebar-list-title" style="color: var(--color-base)"><a href="/wiki/Types_of_earthquake" title="Types of earthquake">Types</a></div><div class="sidebar-list-content mw-collapsible-content hlist"> <ul><li><a href="/wiki/Mainshock" title="Mainshock">Mainshock</a></li> <li><a href="/wiki/Foreshock" title="Foreshock">Foreshock</a></li> <li><a href="/wiki/Aftershock" title="Aftershock">Aftershock</a></li> <li><a href="/wiki/Blind_thrust_earthquake" title="Blind thrust earthquake">Blind thrust</a></li> <li><a href="/wiki/Doublet_earthquake" title="Doublet earthquake">Doublet</a></li> <li><a href="/wiki/Interplate_earthquake" title="Interplate earthquake">Interplate</a></li> <li><a href="/wiki/Intraplate_earthquake" title="Intraplate earthquake">Intraplate</a></li> <li><a href="/wiki/Megathrust_earthquake" title="Megathrust earthquake">Megathrust</a></li> <li><a href="/wiki/Remotely_triggered_earthquakes" title="Remotely triggered earthquakes">Remotely triggered</a></li> <li><a href="/wiki/Slow_earthquake" title="Slow earthquake">Slow</a></li> <li><a href="/wiki/Submarine_earthquake" title="Submarine earthquake">Submarine</a></li> <li><a href="/wiki/Supershear_earthquake" title="Supershear earthquake">Supershear</a></li> <li><a href="/wiki/Tsunami_earthquake" title="Tsunami earthquake">Tsunami</a></li> <li><a href="/wiki/Earthquake_swarm" title="Earthquake swarm">Earthquake swarm</a></li></ul></div></div></td> </tr><tr><td class="sidebar-content"> <div class="sidebar-list mw-collapsible mw-collapsed"><div class="sidebar-list-title" style="color: var(--color-base)">Causes</div><div class="sidebar-list-content mw-collapsible-content hlist"> <ul><li><a href="/wiki/Fault_(geology)" title="Fault (geology)">Fault movement</a></li> <li><a href="/wiki/Volcano_tectonic_earthquake" title="Volcano tectonic earthquake">Volcanism</a></li> <li><a class="mw-selflink selflink">Induced seismicity</a></li></ul></div></div></td> </tr><tr><td class="sidebar-content"> <div class="sidebar-list mw-collapsible mw-collapsed"><div class="sidebar-list-title" style="color: var(--color-base)">Characteristics</div><div class="sidebar-list-content mw-collapsible-content hlist"> <ul><li><a href="/wiki/Epicenter" title="Epicenter">Epicenter</a></li> <li><a href="/wiki/Epicentral_distance" title="Epicentral distance">Epicentral distance</a></li> <li><a href="/wiki/Hypocenter" title="Hypocenter">Hypocenter</a></li> <li><a href="/wiki/Shadow_zone" title="Shadow zone">Shadow zone</a></li> <li><a href="/wiki/Seismic_wave" title="Seismic wave">Seismic waves</a></li> <li><a href="/wiki/P_wave" title="P wave">P wave</a></li> <li><a href="/wiki/S_wave" title="S wave">S wave</a></li></ul></div></div></td> </tr><tr><td class="sidebar-content"> <div class="sidebar-list mw-collapsible mw-collapsed"><div class="sidebar-list-title" style="color: var(--color-base)">Measurement</div><div class="sidebar-list-content mw-collapsible-content hlist"> <ul><li><a href="/wiki/Seismometer" title="Seismometer">Seismometer</a></li> <li><a href="/wiki/Seismic_magnitude_scales" title="Seismic magnitude scales">Seismic magnitude scales</a></li> <li><a href="/wiki/Seismic_intensity_scales" title="Seismic intensity scales">Seismic intensity scales</a></li></ul></div></div></td> </tr><tr><td class="sidebar-content"> <div class="sidebar-list mw-collapsible mw-collapsed"><div class="sidebar-list-title" style="color: var(--color-base)"><a href="/wiki/Earthquake_prediction" title="Earthquake prediction">Prediction</a></div><div class="sidebar-list-content 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regions">Flinn–Engdahl regions</a></li> <li><a href="/wiki/Earthquake_engineering" title="Earthquake engineering">Earthquake engineering</a></li> <li><a href="/wiki/Seismite" title="Seismite">Seismite</a></li> <li><a href="/wiki/Seismology" title="Seismology">Seismology</a></li></ul></div></div></td> </tr><tr><td class="sidebar-below hlist"> <ul><li><a href="/wiki/Portal:Earth_sciences" title="Portal:Earth sciences">Earth Sciences Portal</a></li></ul> <ul><li><a href="/wiki/Category:Earthquakes" title="Category:Earthquakes">Category</a></li> <li><a href="/wiki/Index_of_geology_articles" title="Index of geology articles">Related topics</a></li></ul></td></tr><tr><td class="sidebar-navbar" style="border-top:1px solid #aaa;"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1129693374"><style data-mw-deduplicate="TemplateStyles:r1239400231">.mw-parser-output .navbar{display:inline;font-size:88%;font-weight:normal}.mw-parser-output .navbar-collapse{float:left;text-align:left}.mw-parser-output .navbar-boxtext{word-spacing:0}.mw-parser-output .navbar ul{display:inline-block;white-space:nowrap;line-height:inherit}.mw-parser-output .navbar-brackets::before{margin-right:-0.125em;content:"[ "}.mw-parser-output .navbar-brackets::after{margin-left:-0.125em;content:" ]"}.mw-parser-output .navbar li{word-spacing:-0.125em}.mw-parser-output .navbar a>span,.mw-parser-output .navbar a>abbr{text-decoration:inherit}.mw-parser-output .navbar-mini abbr{font-variant:small-caps;border-bottom:none;text-decoration:none;cursor:inherit}.mw-parser-output .navbar-ct-full{font-size:114%;margin:0 7em}.mw-parser-output .navbar-ct-mini{font-size:114%;margin:0 4em}html.skin-theme-clientpref-night .mw-parser-output .navbar li a abbr{color:var(--color-base)!important}@media(prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .navbar li a abbr{color:var(--color-base)!important}}@media print{.mw-parser-output .navbar{display:none!important}}</style><div class="navbar plainlinks hlist navbar-mini"><ul><li class="nv-view"><a href="/wiki/Template:Earthquakes" title="Template:Earthquakes"><abbr title="View this template">v</abbr></a></li><li class="nv-talk"><a href="/wiki/Template_talk:Earthquakes" title="Template talk:Earthquakes"><abbr title="Discuss this template">t</abbr></a></li><li class="nv-edit"><a href="/wiki/Special:EditPage/Template:Earthquakes" title="Special:EditPage/Template:Earthquakes"><abbr title="Edit this template">e</abbr></a></li></ul></div></td></tr></tbody></table> Induced seismicity is typically <a href="/wiki/Earthquake" title="Earthquake">earthquakes</a> and tremors that are caused by <a href="/wiki/Human" title="Human">human</a> activity that alters the stresses and strains on <a href="/wiki/Earth%27s_crust" title="Earth's crust">Earth's crust</a>. Most induced seismicity is of a low <a href="/wiki/Seismic_magnitude_scales" title="Seismic magnitude scales">magnitude</a>. A few sites regularly have larger quakes, such as <a href="/wiki/The_Geysers" title="The Geysers">The Geysers</a> geothermal plant in California which averaged two M4 events and 15 M3 events every year from 2004 to 2009.<a href="#cite_note-andersonsprings_2009-1">[1]</a> <a href="/wiki/The_Human-Induced_Earthquake_Database" title="The Human-Induced Earthquake Database">The Human-Induced Earthquake Database</a> (HiQuake) documents all reported cases of induced seismicity proposed on scientific grounds and is the most complete compilation of its kind.<a href="#cite_note-2">[2]</a><a href="#cite_note-3">[3]</a> Results of ongoing multi-year research on induced earthquakes by the <a href="/wiki/United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a> (USGS) published in 2015 suggested that most of the significant earthquakes in Oklahoma, such as the 1952 magnitude 5.7 El Reno earthquake may have been induced by deep injection of wastewater by the oil industry. A huge number of seismic events in oil and gas extraction states like Oklahoma is caused by increasing the volume of wastewater injection that is generated as part of the extraction process.<a href="#cite_note-4">[4]</a> "Earthquake rates have recently increased markedly in multiple areas of the Central and Eastern United States (CEUS), especially since 2010, and scientific studies have linked the majority of this increased activity to wastewater injection in deep disposal wells."<a href="#cite_note-usgs_2015-5">[5]</a><a href="#cite_note-Ellsworth_2013-6">[6]</a><a href="#cite_note-7">[7]</a><a href="#cite_note-8">[8]</a><a href="#cite_note-9">[9]</a><a href="#cite_note-USGS_2016_forecast-10">[10]</a>: 2 <a href="#cite_note-Geology_2013-11">[11]</a> Induced seismicity can also be caused by the injection of carbon dioxide as the storage step of carbon capture and storage, which aims to sequester carbon dioxide captured from fossil fuel production or other sources in Earth's crust as a means of <a href="/wiki/Climate_change_mitigation" title="Climate change mitigation">climate change mitigation</a>. This effect has been observed in Oklahoma and Saskatchewan.<a href="#cite_note-:0-12">[12]</a> Though safe practices and existing technologies can be utilized to reduce the risk of induced seismicity due to injection of carbon dioxide, the risk is still significant if the storage is large in scale. The consequences of the induced seismicity could disrupt pre-existing faults in the Earth's crust as well as compromise the seal integrity of the storage locations.<a href="#cite_note-:1-13">[13]</a> The <a href="/wiki/Seismic_hazard" title="Seismic hazard">seismic hazard</a> from induced seismicity can be assessed using similar techniques as for natural seismicity, although accounting for non-stationary seismicity.<a href="#cite_note-gupta_risk-14">[14]</a><a href="#cite_note-Bourne_2015_1721–1738-15">[15]</a> It appears that earthquake shaking from induced earthquakes may be similar to that observed in natural tectonic earthquakes,<a href="#cite_note-16">[16]</a><a href="#cite_note-17">[17]</a> or may have higher shaking at shorter distances.<a href="#cite_note-gupta_gm-18">[18]</a> This means that <a href="/wiki/Seismology#Engineering_seismology" title="Seismology">ground-motion models</a> derived from recordings of natural earthquakes, which are often more numerous in strong-motion databases<a href="#cite_note-19">[19]</a> than data from induced earthquakes, may be used with minor adjustments. Subsequently, a risk assessment can be performed, taking into account the increased seismic hazard and the <a href="/wiki/Earthquake_engineering" title="Earthquake engineering">vulnerability</a> of the exposed elements at risk (e.g. local population and the building stock).<a href="#cite_note-gupta_risk-14">[14]</a><a href="#cite_note-20">[20]</a> Finally, the risk can, theoretically at least, be mitigated, either through reductions to the hazard<a href="#cite_note-21">[21]</a><a href="#cite_note-22">[22]</a> or a reduction to the exposure or the vulnerability.<a href="#cite_note-23">[23]</a> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Causes">Causes</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=1" title="Edit section: Causes">edit</a>]</div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Fluids_and_faults.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/3/35/Fluids_and_faults.jpg/290px-Fluids_and_faults.jpg" decoding="async" width="290" height="185" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/3/35/Fluids_and_faults.jpg/435px-Fluids_and_faults.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/3/35/Fluids_and_faults.jpg/580px-Fluids_and_faults.jpg 2x" data-file-width="928" data-file-height="593" /></a><figcaption>Diagram showing the effects that fluid injection and withdrawal can have on nearby faults can cause induced seismicity.</figcaption></figure> There are many ways in which induced seismicity has been seen to occur. In the 2010s, some energy technologies that inject or extract fluid from the <a href="/wiki/Earth" title="Earth">Earth</a>, such as oil and gas extraction and geothermal energy development, have been found or suspected to cause seismic events. Some energy technologies also produce wastes that may be managed through disposal or storage by injection deep into the ground. For example, waste water from oil and gas production and <a href="/wiki/Carbon_dioxide" title="Carbon dioxide">carbon dioxide</a> from a variety of industrial processes may be managed through underground injection.[<a href="/wiki/Wikipedia:Citation_needed" title="Wikipedia:Citation needed">citation needed</a>] <div class="mw-heading mw-heading3"><h3 id="Artificial_lakes">Artificial lakes</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=2" title="Edit section: Artificial lakes">edit</a>]</div> <style data-mw-deduplicate="TemplateStyles:r1251242444">.mw-parser-output .ambox{border:1px solid #a2a9b1;border-left:10px solid #36c;background-color:#fbfbfb;box-sizing:border-box}.mw-parser-output .ambox+link+.ambox,.mw-parser-output .ambox+link+style+.ambox,.mw-parser-output .ambox+link+link+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+style+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+link+.ambox{margin-top:-1px}html body.mediawiki .mw-parser-output .ambox.mbox-small-left{margin:4px 1em 4px 0;overflow:hidden;width:238px;border-collapse:collapse;font-size:88%;line-height:1.25em}.mw-parser-output .ambox-speedy{border-left:10px solid #b32424;background-color:#fee7e6}.mw-parser-output .ambox-delete{border-left:10px solid #b32424}.mw-parser-output .ambox-content{border-left:10px solid #f28500}.mw-parser-output .ambox-style{border-left:10px solid #fc3}.mw-parser-output .ambox-move{border-left:10px solid #9932cc}.mw-parser-output .ambox-protection{border-left:10px solid #a2a9b1}.mw-parser-output .ambox .mbox-text{border:none;padding:0.25em 0.5em;width:100%}.mw-parser-output .ambox .mbox-image{border:none;padding:2px 0 2px 0.5em;text-align:center}.mw-parser-output .ambox .mbox-imageright{border:none;padding:2px 0.5em 2px 0;text-align:center}.mw-parser-output .ambox .mbox-empty-cell{border:none;padding:0;width:1px}.mw-parser-output .ambox .mbox-image-div{width:52px}@media(min-width:720px){.mw-parser-output .ambox{margin:0 10%}}@media print{body.ns-0 .mw-parser-output .ambox{display:none!important}}</style><table class="box-More_citations_needed_section plainlinks metadata ambox ambox-content ambox-Refimprove" role="presentation"><tbody><tr><td class="mbox-image"><div class="mbox-image-div"><a href="/wiki/File:Question_book-new.svg" class="mw-file-description"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/9/99/Question_book-new.svg/50px-Question_book-new.svg.png" decoding="async" width="50" height="39" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/9/99/Question_book-new.svg/75px-Question_book-new.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/9/99/Question_book-new.svg/100px-Question_book-new.svg.png 2x" data-file-width="512" data-file-height="399" /></a></div></td><td class="mbox-text"><div class="mbox-text-span">This section needs additional citations for <a href="/wiki/Wikipedia:Verifiability" title="Wikipedia:Verifiability">verification</a>. Please help <a href="/wiki/Special:EditPage/Induced_seismicity" title="Special:EditPage/Induced seismicity">improve this article</a> by <a href="/wiki/Help:Referencing_for_beginners" title="Help:Referencing for beginners">adding citations to reliable sources</a> in this section. Unsourced material may be challenged and removed. (January 2021) (<a href="/wiki/Help:Maintenance_template_removal" title="Help:Maintenance template removal">Learn how and when to remove this message</a>)</div></td></tr></tbody></table> The column of water in a large and deep <a href="/wiki/Lake#Artificial_lakes" title="Lake">artificial lake</a> alters in-situ stress along an existing fault or fracture. In these reservoirs, the weight of the water column can significantly change the stress on an underlying fault or fracture by increasing the total stress through direct loading, or decreasing the effective stress through the increased pore water pressure. This significant change in stress can lead to sudden movement along the fault or fracture, resulting in an earthquake.<a href="#cite_note-24">[24]</a> Reservoir-induced seismic events can be relatively large compared to other forms of induced seismicity. Though understanding of reservoir-induced seismic activity is very limited, it has been noted that seismicity appears to occur on dams with heights larger than 330 feet (100 m). The extra water pressure created by large reservoirs is the most accepted explanation for the seismic activity.<a href="#cite_note-25">[25]</a> When the reservoirs are filled or drained, induced seismicity can occur immediately or with a small time lag. The first case of reservoir-induced seismicity occurred in 1932 in Algeria's <a href="/wiki/Oued_Fodda" title="Oued Fodda">Oued Fodda</a> Dam. <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Koyna-Dam.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/2/2d/Koyna-Dam.jpg/220px-Koyna-Dam.jpg" decoding="async" width="220" height="143" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/2/2d/Koyna-Dam.jpg/330px-Koyna-Dam.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/2/2d/Koyna-Dam.jpg/440px-Koyna-Dam.jpg 2x" data-file-width="500" data-file-height="326" /></a><figcaption>The largest earthquake attributed to reservoir-induced seismicity occurred at <a href="/wiki/Koyna_Dam" title="Koyna Dam">Koyna Dam</a></figcaption></figure> The 6.3 magnitude <a href="/wiki/1967_Koynanagar_earthquake" title="1967 Koynanagar earthquake">1967 Koynanagar earthquake</a> occurred in <a href="/wiki/Maharashtra" title="Maharashtra">Maharashtra</a>, <a href="/wiki/India" title="India">India</a> with its <a href="/wiki/Epicenter" title="Epicenter">epicenter</a>, <a href="/wiki/Foreshock" title="Foreshock">fore-</a> and <a href="/wiki/Aftershock" title="Aftershock">aftershocks</a> all located near or under the <a href="/wiki/Koyna_Dam_reservoir" class="mw-redirect" title="Koyna Dam reservoir">Koyna Dam reservoir</a>.<a href="#cite_note-26">[26]</a> 180 people died and 1,500 were left injured. The effects of the earthquake were felt 140 mi (230 km) away in Bombay with tremors and power outages. During the beginnings of the <a href="/wiki/Vajont_Dam" title="Vajont Dam">Vajont Dam</a> in Italy, there were seismic shocks recorded during its initial fill. After a landslide almost filled the reservoir in 1963, causing a massive flooding and around 2,000 deaths, it was drained and consequently seismic activity was almost non-existent. On August 1, 1975, a magnitude 6.1 earthquake at <a href="/wiki/Oroville,_California" title="Oroville, California">Oroville</a>, <a href="/wiki/California" title="California">California</a>, was attributed to seismicity from a large earth-fill <a href="/wiki/Oroville_Dam" title="Oroville Dam">dam</a> and <a href="/wiki/Lake_Oroville" title="Lake Oroville">reservoir</a> recently constructed and filled. The filling of the <a href="/wiki/Katse_Dam" title="Katse Dam">Katse Dam</a> in <a href="/wiki/Lesotho" title="Lesotho">Lesotho</a>, and the <a href="/wiki/Nurek_Dam" title="Nurek Dam">Nurek Dam</a> in <a href="/wiki/Tajikistan" title="Tajikistan">Tajikistan</a> is an example.<a href="#cite_note-27">[27]</a> In <a href="/wiki/Zambia" title="Zambia">Zambia</a>, <a href="/wiki/Kariba_Lake" class="mw-redirect" title="Kariba Lake">Kariba Lake</a> may have provoked similar effects. The <a href="/wiki/2008_Sichuan_earthquake" title="2008 Sichuan earthquake">2008 Sichuan earthquake</a>, which caused approximately 68,000 deaths, is another possible example. An article in <a href="/wiki/Science_(journal)" title="Science (journal)">Science</a> suggested that the construction and filling of the <a href="/wiki/Zipingpu_Dam" title="Zipingpu Dam">Zipingpu Dam</a> may have triggered the earthquake.<a href="#cite_note-28">[28]</a><a href="#cite_note-29">[29]</a><a href="#cite_note-30">[30]</a> Some experts worry that the <a href="/wiki/Three_Gorges_Dam" title="Three Gorges Dam">Three Gorges Dam</a> in <a href="/wiki/China" title="China">China</a> may cause an increase in the frequency and intensity of earthquakes.<a href="#cite_note-31">[31]</a> <div class="mw-heading mw-heading3"><h3 id="Mining">Mining</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=3" title="Edit section: Mining">edit</a>]</div> <a href="/wiki/Mining" title="Mining">Mining</a> affects the <a href="/wiki/Stress_(mechanics)" title="Stress (mechanics)">stress</a> state of the surrounding rock mass, often causing observable <a href="/wiki/Deformation_(mechanics)" class="mw-redirect" title="Deformation (mechanics)">deformation</a> and <a href="/wiki/Earthquake" title="Earthquake">seismic activity</a>. A small portion of mining-induced events are associated with damage to mine workings and pose a risk to mine workers.<a href="#cite_note-:2-32">[32]</a> These events are known as <a href="/wiki/Rock_burst" title="Rock burst">rock bursts</a> in <a href="/wiki/Underground_mining_(hard_rock)" class="mw-redirect" title="Underground mining (hard rock)">hard rock mining</a>, or as <a href="/wiki/Coal_mine_bump" title="Coal mine bump">bumps</a> in <a href="/wiki/Coal_mining#Underground_mining" title="Coal mining">underground coal mining</a>. A mine's propensity to burst or bump depends primarily on depth, mining method, extraction sequence and geometry, and the material properties of the surrounding rock. Many underground hardrock mines operate seismic monitoring networks in order to manage bursting risks, and guide mining practices.<a href="#cite_note-33">[33]</a> Seismic networks have recorded a variety of mining-related seismic sources including: <ul><li>Shear slip events (similar to <a href="/wiki/Earthquake" title="Earthquake">tectonic earthquakes</a>) which are thought to have been triggered by mining activity. Notable examples include the 1980 Bełchatów earthquake<a href="#cite_note-34">[34]</a> and the <a href="/wiki/2014_Orkney_earthquake" title="2014 Orkney earthquake">2014 Orkney earthquake</a>.</li> <li>Implosional events associated with mine collapses. The <a href="/wiki/Crandall_Canyon_Mine#Mining_accidents" title="Crandall Canyon Mine">2007 Crandall Canyon mine collapse</a> and the Solvay Mine Collapse<a href="#cite_note-35">[35]</a> are examples of these.</li> <li>Explosions associated with routine mining practices, such as <a href="/wiki/Drilling_and_blasting" title="Drilling and blasting">drilling and blasting</a>, and unintended explosions such as the <a href="/wiki/Sago_Mine_disaster" title="Sago Mine disaster">Sago mine Disaster</a>.<a href="#cite_note-36">[36]</a> Explosions are generally not considered "induced" events since they are caused entirely by chemical payloads. Most earthquake monitoring agencies take careful measures to identify explosions<a href="#cite_note-37">[37]</a> and exclude them from earthquake catalogs.</li> <li><a href="/wiki/Fracture_mechanics" title="Fracture mechanics">Fracture formation</a> near the surface of excavations, which are usually small magnitude events only detected by dense in-mine networks.<a href="#cite_note-:2-32">[32]</a></li> <li><a href="/wiki/Landslide" title="Landslide">Slope failures</a>, the largest example being the <a href="/wiki/Bingham_Canyon_Mine#Landslides" title="Bingham Canyon Mine">Bingham Canyon Landslide</a>.<a href="#cite_note-38">[38]</a></li></ul> <div class="mw-heading mw-heading3"><h3 id="Waste_disposal_wells">Waste disposal wells</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=4" title="Edit section: Waste disposal wells">edit</a>]</div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Cumulative_induced_seismicity.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/79/Cumulative_induced_seismicity.png/280px-Cumulative_induced_seismicity.png" decoding="async" width="280" height="210" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/79/Cumulative_induced_seismicity.png/420px-Cumulative_induced_seismicity.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/79/Cumulative_induced_seismicity.png/560px-Cumulative_induced_seismicity.png 2x" data-file-width="1167" data-file-height="876" /></a><figcaption>Cumulative number of earthquakes in the central U.S. The red cluster at the center of the map shows an area in and around Oklahoma which experienced the largest increase in activity since 2009.</figcaption></figure> <style data-mw-deduplicate="TemplateStyles:r1236090951">.mw-parser-output .hatnote{font-style:italic}.mw-parser-output div.hatnote{padding-left:1.6em;margin-bottom:0.5em}.mw-parser-output .hatnote i{font-style:normal}.mw-parser-output .hatnote+link+.hatnote{margin-top:-0.5em}@media print{body.ns-0 .mw-parser-output .hatnote{display:none!important}}</style><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Injection_well#Injection-induced_earthquakes" title="Injection well">Injection well § Injection-induced earthquakes</a></div> Injecting liquids into waste disposal wells, most commonly in disposing of <a href="/wiki/Produced_water" title="Produced water">produced water</a> from oil and natural gas wells, has been known to cause earthquakes. This high-saline water is usually pumped into salt water disposal (SWD) wells. The resulting increase in subsurface pore pressure can trigger movement along faults, resulting in earthquakes.<a href="#cite_note-39">[39]</a><a href="#cite_note-40">[40]</a> One of the first known examples was from the <a href="/wiki/Rocky_Mountain_Arsenal" title="Rocky Mountain Arsenal">Rocky Mountain Arsenal</a>, northeast of <a href="/wiki/Denver" title="Denver">Denver</a>. In 1961, waste water was injected into deep strata, and this was later found to have caused a series of earthquakes.<a href="#cite_note-41">[41]</a> The <a href="/wiki/2011_Oklahoma_earthquake" title="2011 Oklahoma earthquake">2011 Oklahoma earthquake</a> near <a href="/wiki/Prague_Oklahoma" class="mw-redirect" title="Prague Oklahoma">Prague</a>, of magnitude 5.8,<a href="#cite_note-42">[42]</a> occurred after 20 years of injecting waste water into porous deep formations at increasing pressures and saturation.<a href="#cite_note-NYT032813-43">[43]</a> On September 3, 2016, an even stronger earthquake with a magnitude of 5.8 occurred near <a href="/wiki/Pawnee,_Oklahoma" title="Pawnee, Oklahoma">Pawnee, Oklahoma</a>, followed by nine aftershocks between magnitudes 2.6 and 3.6 within <style data-mw-deduplicate="TemplateStyles:r1154941027">.mw-parser-output .frac{white-space:nowrap}.mw-parser-output .frac .num,.mw-parser-output .frac .den{font-size:80%;line-height:0;vertical-align:super}.mw-parser-output .frac .den{vertical-align:sub}.mw-parser-output .sr-only{border:0;clip:rect(0,0,0,0);clip-path:polygon(0px 0px,0px 0px,0px 0px);height:1px;margin:-1px;overflow:hidden;padding:0;position:absolute;width:1px}</style>3+1⁄2 hours. Tremors were felt as far away as <a href="/wiki/Memphis,_Tennessee" title="Memphis, Tennessee">Memphis, Tennessee</a>, and <a href="/wiki/Gilbert,_Arizona" title="Gilbert, Arizona">Gilbert, Arizona</a>. <a href="/wiki/Mary_Fallin" title="Mary Fallin">Mary Fallin</a>, the Oklahoma governor, declared a local emergency and shutdown orders for local disposal wells were ordered by the Oklahoma Corporation Commission.<a href="#cite_note-44">[44]</a><a href="#cite_note-45">[45]</a> Results of ongoing multi-year research on induced earthquakes by the <a href="/wiki/United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a> (USGS) published in 2015 suggested that most of the significant earthquakes in Oklahoma, such as the 1952 magnitude 5.5 El Reno earthquake may have been induced by deep injection of waste water by the oil industry.<a href="#cite_note-usgs_2015-5">[5]</a> Prior to April 2015 however, the Oklahoma Geological Survey's position was that the quake was most likely due to natural causes and was not triggered by waste injection.<a href="#cite_note-46">[46]</a> This was <a href="/wiki/Oklahoma_earthquake_swarms_(2009%E2%80%93present)" title="Oklahoma earthquake swarms (2009–present)">one of many earthquakes</a> which have affected the Oklahoma region. Since 2009, earthquakes have become hundreds of times more common in Oklahoma with magnitude 3 events increasing from 1 or 2 per year to 1 or 2 per day.<a href="#cite_note-47">[47]</a> On April 21, 2015, the Oklahoma Geological Survey released a statement reversing its stance on induced earthquakes in Oklahoma: "The OGS considers it very likely that the majority of recent earthquakes, particularly those in central and north-central Oklahoma, are triggered by the injection of produced water in disposal wells."<a href="#cite_note-48">[48]</a> <div class="mw-heading mw-heading3"><h3 id="Hydrocarbon_extraction_and_storage">Hydrocarbon extraction and storage</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=5" title="Edit section: Hydrocarbon extraction and storage">edit</a>]</div> Large-scale fossil fuel extraction can generate earthquakes.<a href="#cite_note-49">[49]</a><a href="#cite_note-50">[50]</a> Induced seismicity can be also related to underground gas storage operations. The 2013 September–October seismic sequence occurred 21 km off the coast of the Valencia Gulf (Spain) is probably the best known case of induced seismicity related to Underground Gas Storage operations (the Castor Project). In September 2013, after the injection operations started, the Spanish seismic network recorded a sudden increase of seismicity. More than 1,000 events with magnitudes (<a href="/wiki/Seismic_magnitude_scales#ML" title="Seismic magnitude scales"><style data-mw-deduplicate="TemplateStyles:r1038841319">'"`UNIQ--templatestyles-00000043-QINU`"'</style>ML</a>) between 0.7 and 4.3 (the largest earthquake ever associated with gas storage operations) and located close the injection platform were recorded in about 40 days.<a href="#cite_note-51">[51]</a><a href="#cite_note-52">[52]</a> Due to the significant population concern the Spanish Government halted the operations. By the end of 2014, the Spanish government definitively terminated the concession of the UGS plant. Since January 2015 about 20 people who took part in the transaction and approval of the Castor Project were indicted.[<a href="/wiki/Wikipedia:Citation_needed" title="Wikipedia:Citation needed">citation needed</a>] <div class="mw-heading mw-heading3"><h3 id="Groundwater_extraction">Groundwater extraction</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=6" title="Edit section: Groundwater extraction">edit</a>]</div> The changes in crustal stress patterns caused by the large scale extraction of groundwater has been shown to trigger earthquakes, as in the case of the <a href="/wiki/2011_Lorca_earthquake" title="2011 Lorca earthquake">2011 Lorca earthquake</a>.<a href="#cite_note-González-53">[53]</a> <div class="mw-heading mw-heading3"><h3 id="Geothermal_energy">Geothermal energy</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=7" title="Edit section: Geothermal energy">edit</a>]</div> <a href="/wiki/Enhanced_geothermal_systems" class="mw-redirect" title="Enhanced geothermal systems">Enhanced geothermal systems</a> (EGS), a new type of <a href="/wiki/Geothermal_power" title="Geothermal power">geothermal power</a> technology that does not require natural convective hydrothermal resources, are known to be associated with induced seismicity. EGS involves pumping fluids at pressure to enhance or create permeability through the use of hydraulic fracturing techniques. Hot dry rock (HDR) EGS actively creates geothermal resources through hydraulic stimulation. Depending on the rock properties, and on injection pressures and fluid volume, the reservoir rock may respond with tensile failure, as is common in the oil and gas industry, or with shear failure of the rock's existing joint set, as is thought to be the main mechanism of reservoir growth in EGS efforts.<a href="#cite_note-54">[54]</a> HDR and EGS systems are currently being developed and tested in Soultz-sous-Forêts (France), Desert Peak and <a href="/wiki/The_Geysers" title="The Geysers">the Geysers</a> (U.S.), Landau (Germany), and Paralana and Cooper Basin (Australia). Induced seismicity events at the Geysers geothermal field in California has been strongly correlated with injection data.<a href="#cite_note-55">[55]</a> The test site at Basel, Switzerland, has been shut down due to induced seismic events. In November 2017 a Mw 5.5 struck the city of Pohang (South Korea) injuring several people and causing extensive damage. The proximity of the seismic sequence to an EGS site, where stimulation operations had taken place only a few months before the earthquake, raised the possibility that this earthquake had been anthropogenic. According to two different studies it seems plausible that the <a href="/wiki/2017_Pohang_earthquake" title="2017 Pohang earthquake">Pohang earthquake</a> was induced by EGS operations.<a href="#cite_note-56">[56]</a><a href="#cite_note-57">[57]</a> <table class="wikitable"> <caption>Largest Events at EGS Sites Worldwide<a href="#cite_note-58">[58]</a> </caption> <tbody><tr align="center"> <th>Site </th> <th>Maximum Magnitude </th></tr> <tr align="center"> <td>Pohang, South Korea </td> <td>5.5 </td></tr> <tr align="center"> <td>The Geysers, United States </td> <td>4.6 </td></tr> <tr align="center"> <td>Cooper Basin, Australia </td> <td>3.7 </td></tr> <tr align="center"> <td>Basel, Switzerland </td> <td>3.4 </td></tr> <tr align="center"> <td><a href="/wiki/Rosemanowes_Quarry" title="Rosemanowes Quarry">Rosemanowes Quarry</a>, United Kingdom </td> <td>3.1 </td></tr> <tr align="center"> <td>Soultz-sous-Forêts, France </td> <td>2.9 </td></tr></tbody></table> Researchers at MIT believe that seismicity associated with hydraulic stimulation can be mitigated and controlled through predictive siting and other techniques. With appropriate management, the number and magnitude of induced seismic events can be decreased, significantly reducing the probability of a damaging seismic event.<a href="#cite_note-59">[59]</a> <a href="/wiki/Induced_seismicity_in_Basel" title="Induced seismicity in Basel">Induced seismicity in Basel</a> led to suspension of its HDR project. A seismic hazard evaluation was then conducted, which resulted in the cancellation of the project in December 2009.[<a href="/wiki/Wikipedia:Citation_needed" title="Wikipedia:Citation needed">citation needed</a>] <div class="mw-heading mw-heading3"><h3 id="Hydraulic_fracturing">Hydraulic fracturing</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=8" title="Edit section: Hydraulic fracturing">edit</a>]</div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Hydraulic_fracturing" class="mw-redirect" title="Hydraulic fracturing">Hydraulic fracturing</a></div> <a href="/wiki/Hydraulic_fracturing" class="mw-redirect" title="Hydraulic fracturing">Hydraulic fracturing</a> is a technique in which high-pressure fluid is injected into the low-permeable reservoir rocks in order to induce fractures to increase <a href="/wiki/Hydrocarbon" title="Hydrocarbon">hydrocarbon</a> production.<a href="#cite_note-60">[60]</a> This process is generally associated with <a href="/wiki/Environmental_impact_of_hydraulic_fracturing#Induced_seismicity_from_hydraulic_fracturing" class="mw-redirect" title="Environmental impact of hydraulic fracturing">seismic events</a> that are too small to be felt at the surface (with moment <a href="/wiki/Seismic_magnitude_scales" title="Seismic magnitude scales">magnitudes</a> ranging from −3 to 1), although larger magnitude events are not excluded.<a href="#cite_note-61">[61]</a> For example, several cases of larger magnitude events (M > 4) have been recorded in Canada in the <a href="/wiki/Unconventional_resources" class="mw-redirect" title="Unconventional resources">unconventional resources</a> of <a href="/wiki/Alberta" title="Alberta">Alberta</a> and <a href="/wiki/British_Columbia" title="British Columbia">British Columbia</a>.<a href="#cite_note-62">[62]</a> <div class="mw-heading mw-heading3"><h3 id="Carbon_capture_and_storage">Carbon capture and storage</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=9" title="Edit section: Carbon capture and storage">edit</a>]</div> <div class="mw-heading mw-heading4"><h4 id="Risk_analysis">Risk analysis</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=10" title="Edit section: Risk analysis">edit</a>]</div> Operation of technologies involving long-term geologic storage of waste fluids have been shown to induce seismic activity in nearby areas, and correlation of periods of seismic dormancy with minima in injection volumes and pressures has even been demonstrated for fracking wastewater injection in Youngstown, Ohio.<a href="#cite_note-63">[63]</a> Of particular concern to the viability of carbon dioxide storage from coal-fired power plants and similar endeavors is that the scale of intended CCS projects is much larger in both injection rate and total injection volume than any current or past operation that has already been shown to induce seismicity.<a href="#cite_note-64">[64]</a> As such, extensive modeling must be done of future injection sites in order to assess the risk potential of CCS operations, particularly in relation to the effect of long-term carbon dioxide storage on shale caprock integrity, as the potential for fluid leaks to the surface might be quite high for moderate earthquakes.<a href="#cite_note-:1-13">[13]</a> However, the potential of CCS to induce large earthquakes and CO2 leakage remains a controversial issue.,<a href="#cite_note-65">[65]</a><a href="#cite_note-66">[66]</a><a href="#cite_note-67">[67]</a> <div class="mw-heading mw-heading4"><h4 id="Monitoring">Monitoring</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=11" title="Edit section: Monitoring">edit</a>]</div> Since geological <a href="/wiki/Carbon_sequestration" title="Carbon sequestration">sequestration of carbon</a> dioxide has the potential to induce seismicity, researchers have developed methods to monitor and model the risk of injection-induced seismicity in order to manage better the risks associated with this phenomenon. Monitoring can be conducted with measurements from an instrument such as a <a href="/wiki/Geophone" title="Geophone">geophone</a> to measure the movement of the ground. Generally a network of instruments is used around the site of injection, although many current carbon dioxide injection sites use no monitoring devices. Modelling is an important technique for assessing the potential for induced seismicity and two primary models are used: Physical and numerical. A physical model uses measurements from the early stages of a project to forecast how the project will behave once more carbon dioxide is injected. A numerical model, on the other hand, uses numerical methods to simulate the physics of what is happening within the reservoir. Both modelling and monitoring are useful tools whereby to quantify, understand better and mitigate the risks associated with injection-induced seismicity.<a href="#cite_note-:0-12">[12]</a> <div class="mw-heading mw-heading4"><h4 id="Failure_mechanisms_due_to_fluid_injection">Failure mechanisms due to fluid injection</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=12" title="Edit section: Failure mechanisms due to fluid injection">edit</a>]</div> To assess induced seismicity risks associated with carbon storage, one must understand the mechanisms behind rock failure. The <a href="/wiki/Mohr-Coulomb_theory" class="mw-redirect" title="Mohr-Coulomb theory">Mohr-Coulomb failure criteria</a> describe shear failure on a fault plane.<a href="#cite_note-68">[68]</a> Most generally, failure will happen on existing faults due to several mechanisms: an increase in shear stress, a decrease in normal stress or a <a href="/wiki/Pore_water_pressure" title="Pore water pressure">pore pressure</a> increase.<a href="#cite_note-:0-12">[12]</a> The injection of supercritical CO2 will change the stresses in the reservoir as it expands, causing potential failure on nearby faults. Injection of fluids also increases the pore pressures in the reservoir, triggering slip on existing rock weakness planes. The latter is the most common cause of induced seismicity due to fluid injection.<a href="#cite_note-:0-12">[12]</a> The Mohr-Coulomb failure criteria state that <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \tau _{c}=\tau _{0}+\mu (\sigma _{n}-P)}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <msub> <mi>τ</mi> <mrow class="MJX-TeXAtom-ORD"> <mi>c</mi> </mrow> </msub> <mo>=</mo> <msub> <mi>τ</mi> <mrow class="MJX-TeXAtom-ORD"> <mn>0</mn> </mrow> </msub> <mo>+</mo> <mi>μ</mi> <mo stretchy="false">(</mo> <msub> <mi>σ</mi> <mrow class="MJX-TeXAtom-ORD"> <mi>n</mi> </mrow> </msub> <mo>−</mo> <mi>P</mi> <mo stretchy="false">)</mo> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \tau _{c}=\tau _{0}+\mu (\sigma _{n}-P)}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/86784538c8ac6421d8dfa56acea3eaf092464fae" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.838ex; width:20.312ex; height:2.843ex;" alt="{\displaystyle \tau _{c}=\tau _{0}+\mu (\sigma _{n}-P)}"> with <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \tau _{c}}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <msub> <mi>τ</mi> <mrow class="MJX-TeXAtom-ORD"> <mi>c</mi> </mrow> </msub> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \tau _{c}}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/ea61c9e95de7b5b55eb1ef4b3e03290002e91089" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.671ex; width:1.96ex; height:2.009ex;" alt="{\displaystyle \tau _{c}}"> the critical <a href="/wiki/Shear_stress" title="Shear stress">shear stress</a> leading to failure on a fault, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \tau _{0}}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <msub> <mi>τ</mi> <mrow class="MJX-TeXAtom-ORD"> <mn>0</mn> </mrow> </msub> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \tau _{0}}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/56dad457e274b970f5d98b9dc40bef7f895c7f6f" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.671ex; width:2.07ex; height:2.009ex;" alt="{\displaystyle \tau _{0}}"> the <a href="/wiki/Cohesion_(geology)" title="Cohesion (geology)">cohesive strength</a> along the fault, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \sigma _{n}}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <msub> <mi>σ</mi> <mrow class="MJX-TeXAtom-ORD"> <mi>n</mi> </mrow> </msub> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \sigma _{n}}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/1e4aeaa7d544d1f21afc8c8993cf5e5625ed8f95" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.671ex; width:2.546ex; height:2.009ex;" alt="{\displaystyle \sigma _{n}}"> the normal stress, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \mu }"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>μ</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \mu }</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/9fd47b2a39f7a7856952afec1f1db72c67af6161" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.838ex; width:1.402ex; height:2.176ex;" alt="{\displaystyle \mu }"> the friction coefficient on the fault plane and <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle P}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>P</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle P}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/b4dc73bf40314945ff376bd363916a738548d40a" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:1.745ex; height:2.176ex;" alt="{\displaystyle P}"> the pore pressure within the fault.<a href="#cite_note-:0-12">[12]</a><a href="#cite_note-69">[69]</a> When <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \tau _{c}}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <msub> <mi>τ</mi> <mrow class="MJX-TeXAtom-ORD"> <mi>c</mi> </mrow> </msub> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \tau _{c}}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/ea61c9e95de7b5b55eb1ef4b3e03290002e91089" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.671ex; width:1.96ex; height:2.009ex;" alt="{\displaystyle \tau _{c}}"> is attained, shear failure occurs and an earthquake can be felt. This process can be represented graphically on a <a href="/wiki/Mohr%27s_circle" title="Mohr's circle">Mohr's circle</a>.<a href="#cite_note-:0-12">[12]</a> <div class="mw-heading mw-heading4"><h4 id="Comparison_of_risks_due_to_CCS_versus_other_injection_methods">Comparison of risks due to CCS versus other injection methods</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=13" title="Edit section: Comparison of risks due to CCS versus other injection methods">edit</a>]</div> While there is risk of induced seismicity associated with <a href="/wiki/Carbon_capture_and_storage" title="Carbon capture and storage">carbon capture and storage</a> underground on a large scale, it is currently a much less serious risk than other injection types. Wastewater injection, hydraulic fracturing, and secondary recovery after oil extraction have all contributed significantly more to induced seismic events than carbon capture and storage in the last several years.<a href="#cite_note-70">[70]</a> There have actually not been any major seismic events associated with carbon injection at this point, whereas there have been recorded seismic occurrences caused by the other injection methods. One such example is massively increased induced seismicity in Oklahoma, USA caused by injection of huge volumes of wastewater into the Arbuckle Group sedimentary rock.<a href="#cite_note-71">[71]</a> <div class="mw-heading mw-heading3"><h3 id="Electromagnetic_pulses">Electromagnetic pulses</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=14" title="Edit section: Electromagnetic pulses">edit</a>]</div> It has been shown that high-energy <a href="/wiki/Electromagnetic_pulse" title="Electromagnetic pulse">electromagnetic pulses</a> can trigger the release of energy stored by tectonic movements by increasing the rate of local earthquakes, within 2–6 days after the emission by the EMP generators. The energy released is approximately six orders of magnitude larger than the EM pulses energy.<a href="#cite_note-72">[72]</a> The release of tectonic stress by these relatively small triggered earthquakes equals to 1-17% of the stress released by a strong earthquake in the area.<a href="#cite_note-73">[73]</a> It has been proposed that strong EM impacts could control seismicity as during the periods of the experiments and long time after, the seismicity dynamics were a lot more regular than usual.<a href="#cite_note-74">[74]</a><a href="#cite_note-75">[75]</a> <div class="mw-heading mw-heading2"><h2 id="Risk_analysis_2">Risk analysis</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=15" title="Edit section: Risk analysis">edit</a>]</div> <div class="mw-heading mw-heading3"><h3 id="Risk_factors">Risk factors</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=16" title="Edit section: Risk factors">edit</a>]</div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Seismic_risk" title="Seismic risk">Seismic risk</a></div> Risk is defined as the probability of being impacted from an event in the future. Seismic risk is generally estimated by combining the seismic hazard with the exposure and vulnerability at a site or over a region.<a href="#cite_note-gupta_risk-14">[14]</a> The hazard from earthquakes depends on the proximity to potential earthquake sources, and the rates of occurrence of different magnitude earthquakes for those sources, and the propagation of seismic waves from the sources to the site of interest. Hazard is then represented in terms of the probability of exceeding some level of ground shaking at a site. Earthquake hazards can include ground shaking, liquefaction, surface fault displacement, landslides, tsunamis, and uplift/subsidence for very large events (ML > 6.0). Because induced seismic events, in general, are smaller than ML 5.0 with short durations, the primary concern is ground shaking.<a href="#cite_note-76">[76]</a> <div class="mw-heading mw-heading4"><h4 id="Ground_shaking">Ground shaking</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=17" title="Edit section: Ground shaking">edit</a>]</div> Ground shaking can result in both structural and nonstructural damage<a href="#cite_note-Toward_performance-driven_seismic-77">[77]</a> to buildings and other structures. It is commonly accepted that structural damage to modern engineered structures happens only in earthquakes larger than ML 5.0. In <a href="/wiki/Seismology" title="Seismology">seismology</a> and <a href="/wiki/Earthquake_engineering" title="Earthquake engineering">earthquake engineering</a>, ground shaking can be measured as <a href="/wiki/Peak_ground_velocity" class="mw-redirect" title="Peak ground velocity">peak ground velocity</a> (PGV), <a href="/wiki/Peak_ground_acceleration" title="Peak ground acceleration">peak ground acceleration</a> (PGA) or <a href="/wiki/Spectral_acceleration" title="Spectral acceleration">spectral acceleration</a> (SA) at a building's period of excitation. In regions of historical seismicity where buildings are engineered to withstand seismic forces, moderate structural damage is possible, and very strong shaking can be perceived when PGA is greater than 18-34% of g (the acceleration of gravity).<a href="#cite_note-78">[78]</a> In rare cases, nonstructural damage<a href="#cite_note-Toward_performance-driven_seismic-77">[77]</a> has been reported in earthquakes as small as ML 3.0. For critical facilities like dams and nuclear plants, the acceptable levels of ground shaking is lower than that for buildings.<a href="#cite_note-ASCE-79">[79]</a> <div class="mw-heading mw-heading3"><h3 id="Probabilistic_seismic_hazard_analysis">Probabilistic seismic hazard analysis</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=18" title="Edit section: Probabilistic seismic hazard analysis">edit</a>]</div> Extended reading – <a rel="nofollow" class="external text" href="https://web.stanford.edu/~bakerjw/Publications/Baker_(2008)_Intro_to_PSHA_v1_3.pdf">An Introduction to Probabilistic Seismic Hazard Analysis (PSHA)</a> Probabilistic Seismic Hazard Analysis (PSHA) is a probabilistic framework that accounts for probabilities in earthquake occurrence and the probabilities in ground motion propagation. Using the framework, the probability of exceeding a certain level of ground shaking at a site can be quantified, taking into account all the possible earthquakes (both natural and induced).<a href="#cite_note-:9-80">[80]</a><a href="#cite_note-Stanford.edu-81">[81]</a><a href="#cite_note-82">[82]</a><a href="#cite_note-83">[83]</a> PSHA methodology is used to determine seismic loads for building codes in both the United States and Canada, and increasingly in other parts of the world, as well as protecting dams and nuclear plants from the damage of seismic events.<a href="#cite_note-ASCE-79">[79]</a><a href="#cite_note-:9-80">[80]</a><a href="#cite_note-84">[84]</a> <div class="mw-heading mw-heading3"><h3 id="Calculating_Seismic_Risk">Calculating Seismic Risk</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=19" title="Edit section: Calculating Seismic Risk">edit</a>]</div> <div class="mw-heading mw-heading4"><h4 id="Earthquake_source_characterization">Earthquake source characterization</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=20" title="Edit section: Earthquake source characterization">edit</a>]</div> Understanding the geological background on the site is a prerequisite for seismic hazard estimation. Formations of the rocks, subsurface structures, locations of faults, state of stresses and other parameters that contribute to possible seismic events are considered. Records of past earthquakes of the site are also taken into account.<a href="#cite_note-Stanford.edu-81">[81]</a> <div class="mw-heading mw-heading4"><h4 id="Recurrence_pattern">Recurrence pattern</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=21" title="Edit section: Recurrence pattern">edit</a>]</div> The magnitudes of earthquakes occurring at a source generally follow the <a href="/wiki/Gutenberg%E2%80%93Richter_law" title="Gutenberg–Richter law">Gutenberg-Richter relation</a> that states that the number of earthquakes decrease exponentially with increase in magnitude, as shown below, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle \log N(\geq M)=a-bM}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>log</mi> <mo>⁡</mo> <mi>N</mi> <mo stretchy="false">(</mo> <mo>≥</mo> <mi>M</mi> <mo stretchy="false">)</mo> <mo>=</mo> <mi>a</mi> <mo>−</mo> <mi>b</mi> <mi>M</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle \log N(\geq M)=a-bM}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/7cb66bffff96626bc7bd3fe9d176dae93588911d" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.838ex; width:22.736ex; height:2.843ex;" alt="{\displaystyle \log N(\geq M)=a-bM}"> where <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle M}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>M</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle M}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/f82cade9898ced02fdd08712e5f0c0151758a0dd" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:2.442ex; height:2.176ex;" alt="{\displaystyle M}"> is the magnitude of seismic events, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle N}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>N</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle N}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/f5e3890c981ae85503089652feb48b191b57aae3" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:2.064ex; height:2.176ex;" alt="{\displaystyle N}"> is the number of events with magnitudes bigger than <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle M}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>M</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle M}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/f82cade9898ced02fdd08712e5f0c0151758a0dd" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:2.442ex; height:2.176ex;" alt="{\displaystyle M}">, <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle a}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>a</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle a}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/ffd2487510aa438433a2579450ab2b3d557e5edc" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:1.23ex; height:1.676ex;" alt="{\displaystyle a}"> is the rate parameter and <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle b}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>b</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle b}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/f11423fbb2e967f986e36804a8ae4271734917c3" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:0.998ex; height:2.176ex;" alt="{\displaystyle b}"> is the slope. <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle a}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>a</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle a}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/ffd2487510aa438433a2579450ab2b3d557e5edc" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:1.23ex; height:1.676ex;" alt="{\displaystyle a}"> and <math xmlns="http://www.w3.org/1998/Math/MathML" alttext="{\displaystyle b}"> <semantics> <mrow class="MJX-TeXAtom-ORD"> <mstyle displaystyle="true" scriptlevel="0"> <mi>b</mi> </mstyle> </mrow> <annotation encoding="application/x-tex">{\displaystyle b}</annotation> </semantics> </math><img src="https://wikimedia.org/api/rest_v1/media/math/render/svg/f11423fbb2e967f986e36804a8ae4271734917c3" class="mwe-math-fallback-image-inline mw-invert skin-invert" aria-hidden="true" style="vertical-align: -0.338ex; width:0.998ex; height:2.176ex;" alt="{\displaystyle b}"> vary for different sources. In the case of natural earthquakes, historical seismicity is used to determine these parameters. Using this relationship, the number and probability of earthquakes exceeding a certain magnitude can be predicted following the assumptions that earthquakes follow a Poisson process.<a href="#cite_note-85">[85]</a><a href="#cite_note-:9-80">[80]</a><a href="#cite_note-86">[86]</a> However, the goal of this analysis is to determine the possibility of future earthquakes. For induced seismicity in contrast to natural seismicity, the earthquake rates change over time as a result of changes in human activity, and hence are quantified as non-stationary processes with varying seismicity rates over time.<a href="#cite_note-87">[87]</a> <div class="mw-heading mw-heading4"><h4 id="Ground_motions">Ground motions</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=22" title="Edit section: Ground motions">edit</a>]</div> At a given site, the ground motion describes the seismic waves that would have been observed at that site with a seismometer. In order to simplify the representation of an entire seismogram, <a href="/wiki/Strong_ground_motion" title="Strong ground motion">PGV (peak ground velocity)</a>, <a href="/wiki/Peak_ground_acceleration" title="Peak ground acceleration">PGA (peak ground acceleration)</a>, <a href="/wiki/Spectral_acceleration" title="Spectral acceleration">spectral acceleration</a> (SA) at different period, earthquake duration, <a href="/wiki/Arias_intensity" title="Arias intensity">arias intensity</a> (IA) are some of the parameters that are used to represent ground shaking. Ground motion propagation from the source to a site for an earthquake of a given magnitude is estimated using ground motion prediction equations (GMPE) that have been developed based on historical records.<a href="#cite_note-88">[88]</a> Since historical records are scarce for induced seismicity, researchers have provided modifications to GMPEs for natural earthquakes in order to apply them to indced earthquakes.<a href="#cite_note-gupta_gm-18">[18]</a><a href="#cite_note-89">[89]</a> <div class="mw-heading mw-heading4"><h4 id="Seismic_hazard">Seismic hazard</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=23" title="Edit section: Seismic hazard">edit</a>]</div> The PSHA framework uses the distributions of earthquake magnitudes and ground motion propagation to estimate the seismic hazard – the probability of exceeding a certain level of ground shaking (PGA, PGV, SA, IA, etc.) in the future.<a href="#cite_note-90">[90]</a> Depending on the complexity of the probability distributions, either numerical methods or simulations (such as, <a href="/wiki/Monte_Carlo_method" title="Monte Carlo method">Monte Carlo method</a>) may be used to estimate seismic hazard.<a href="#cite_note-:9-80">[80]</a><a href="#cite_note-Bourne_2015_1721–1738-15">[15]</a> In the case of induced seismicity, the seismic hazard is not constant, but varies with time due to changes in the underlying seismicity rates.<a href="#cite_note-gupta_risk-14">[14]</a> <div class="mw-heading mw-heading4"><h4 id="Exposure_and_vulnerability">Exposure and vulnerability</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=24" title="Edit section: Exposure and vulnerability">edit</a>]</div> In order to estimate seismic risk, the hazard is combined with the exposure and vulnerability at a site or in a region. For example, if an earthquake occurs where there are no humans or structures, there would be no human impacts despite any level of seismic hazard. Exposure is defined as the set of entities (such as, buildings and people) that exist at a given site or a region. Vulnerability is defined as the potential of impact to those entities, for example, structural or non-structural damage to a building, and loss of well-being and life for people. Vulnerability can also be represented probabilistically using vulnerability or fragility functions.<a href="#cite_note-91">[91]</a><a href="#cite_note-92">[92]</a> A vulnerability or fragility function specifies the probability of impact at different levels of ground shaking. In regions like Oklahoma without a lot of historical natural seismicity, structures are not engineered to withstand seismic forces, and as a result are more vulnerable even at low levels of ground shaking, as compared to structures in tectonic regions like California and Japan. <div class="mw-heading mw-heading4"><h4 id="Seismic_risk">Seismic risk</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=25" title="Edit section: Seismic risk">edit</a>]</div> Seismic risk is defined as the probability of exceeding a certain level of impact in the future. For example, it may estimate the exceedance probability of moderate or more damage to a building in the future. Seismic hazard is combined with the exposure and vulnerability to estimate seismic risk. While numerical methods may be used to estimate risk at one site, simulation-based methods are better suited to estimate seismic risk for a region with a portfolio of entities, in order to correctly account for the correlations in ground shaking, and impacts. In the case of induced seismicity, the seismic risk varies over time due to changes in the seismic hazard.<a href="#cite_note-gupta_risk-14">[14]</a> <div class="mw-heading mw-heading3"><h3 id="Risk_Mitigation">Risk Mitigation</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=26" title="Edit section: Risk Mitigation">edit</a>]</div> Induced seismicity can cause damage to infrastructure and has been documented to damage buildings in Oklahoma.<a href="#cite_note-93">[93]</a> It can also lead to brine and CO2 leakages.<a href="#cite_note-:6-94">[94]</a> It is easier to predict and mitigate seismicity caused by explosions. Common mitigation strategies include constraining the amount of dynamite used in one single explosion and the locations of the explosions. For injection-related induced seismicity, however, it is still difficult to predict when and where induced seismic events will occur, as well as the magnitudes. Since induced seismic events related to fluid injection are unpredictable, it has garnered more attention from the public. Induced seismicity is only part of the chain reaction from industrial activities that worry the public. Impressions toward induced seismicity are very different between different groups of people.<a href="#cite_note-:5-95">[95]</a> The public tends to feel more negatively towards earthquakes caused by human activities than natural earthquakes.<a href="#cite_note-:19-96">[96]</a> Two major parts of public concern are related to the damages to infrastructure and the well-being of humans.<a href="#cite_note-:5-95">[95]</a> Most induced seismic events are below M 2 and are not able to cause any physical damage. Nevertheless, when the seismic events are felt and cause damages or injuries, questions arise from the public whether it is appropriate to conduct oil and gas operations in those areas. Public perceptions may vary based on the population and tolerance of local people. For example, in the seismically active Geysers geothermal area in Northern California, which is a rural area with a relatively small population, the local population tolerates earthquakes up to M 4.5.<a href="#cite_note-97">[97]</a> Actions have been taken by regulators, industry and researchers. On October 6, 2015, people from industry, government, academia, and the public gathered together to discuss how effective it was to implement a traffic light system or protocol in Canada to help manage risks from induced seismicity.<a href="#cite_note-:4-98">[98]</a> Risk assessment and tolerance for induced seismicity, however, is subjective and shaped by different factors like politics, economics, and understanding from the public.<a href="#cite_note-:10-99">[99]</a> Policymakers have to often balance the interests of industry with the interests of the population. In these situations, seismic risk estimation serves as a critical tool for quantifying future risk, and can be used to regulate earthquake-inducing activities until the seismic risk reaches a maximum acceptable level to the population.<a href="#cite_note-gupta_risk-14">[14]</a> <div class="mw-heading mw-heading4"><h4 id="Traffic_Light_System">Traffic Light System</h4>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=27" title="Edit section: Traffic Light System">edit</a>]</div> One of the methods suggested to mitigate seismic risk is a Traffic Light System (TLS), also referred to as Traffic Light Protocol (TLP), which is a calibrated control system that provides continuous and real-time monitoring and management of ground shaking of induced seismicity for specific sites. TLS was first implemented in 2005 in an enhanced geothermal plant in Central America. For oil and gas operations, the most widely implemented one is modified by the system used in the UK. Normally there are two types of TLS – the first one sets different thresholds, usually earthquake local magnitudes (ML) or ground motions from small to large. If the induced seismicity reaches the smaller thresholds, modifications of the operations are implemented by the operators and the regulators are informed. If the induced seismicity reaches the larger thresholds, operations are shut down immediately. The second type of traffic light system sets only one threshold. If this threshold is reached, the operations are halted. This is also called a "stop light system". Thresholds for the traffic light system vary between and within countries, depending on the area. However, the traffic light system is not able to account for future changes in seismicity. It may take time for changes in human activities to mitigate the seismic activity, and it has been observed that some of the largest induced earthquakes have occurred after stopping fluid injection.<a href="#cite_note-100">[100]</a> <table class="wikitable mw-collapsible"> <caption>Traffic Light Systems Around the World<a href="#cite_note-101">[101]</a> </caption> <tbody><tr> <th>Country </th> <th>Location </th> <th>Major Operation </th> <th>TSL </th></tr> <tr> <td>Switzerland </td> <td>Basel </td> <td>Enhanced Geothermal System </td> <td>Operate as planned: PGV < 0.5 mm/s, ML < 2.3, no felt report Inform regulators; no increase in injection rate: PGV ≤ 2.0 mm/s, ML ≥ 2.3, few felt report Reduce injection rate: PGV ≤ 5.0 mm/s, ML ≤ 2.9, many felt reports Suspend pumping; bleeding wells: PGV > 5.0 mm/s, ML > 2.9, generally felt </td></tr> <tr> <td>U.K. </td> <td>Nation-wide </td> <td>Hydraulic Fracturing of Shale Gas </td> <td>Operate as planned: ML < 0 Operate with caution; lower the injection rates; increase monitoring: 0 ≤ ML ≤ 0.5 Suspend operation: ML > 0.5 </td></tr> <tr> <td>U.S.A </td> <td>Colorado </td> <td>Hydraulic Fracturing; Wastewater Disposal </td> <td>Modify the operation: felt at the surface Suspend operation: ML ≥ 4.5 </td></tr> <tr> <td>U.S.A </td> <td>Oklahoma </td> <td>Wastewater Disposal; Hydraulic Fracturing </td> <td>Escalate review of operators' mitigation procedures : ML ≥ 2.5, ≥ 3.0 Suspend the operation : ML ≥ 3.5 </td></tr> <tr> <td>U.S.A </td> <td>Ohio </td> <td>Wastewater Disposal; Hydraulic Fracturing </td> <td>Operate as planned: ML < 1.5 Inform the regulator: ML ≥ 1.5 Modify the operation plan: 2.0 ≤ ML ≤ 2.4 Halt the operations temporarily: ML ≥ 2.5 Suspend the operations: ML ≥ 3.0 </td></tr> <tr> <td>Canada </td> <td>Fox Creek Area, Alberta </td> <td>Hydraulic Fracturing </td> <td>Operate as planned: ML < 2.0 Inform the regulator; implement mitigation plans: 2.0 ≤ ML ≤ 4.0 within 5 km of an injection well Inform the regulator; suspend the operations: ML ≥ 4.0 within 5 km of an injection well </td></tr> <tr> <td>Canada </td> <td>Red Deer Area, Alberta </td> <td>Hydraulic Fracturing </td> <td>Operate as planned: ML < 1.0 Inform the regulator; implement mitigation plans: 1.0 ≤ ML ≤ 3.0 within 5 km of an injection well Inform the regulator; suspend the operations: ML ≥ 3.0 within 5 km of an injection well </td></tr> <tr> <td>Canada </td> <td>British Columbia </td> <td>Hydraulic Fracturing </td> <td>Suspend the operations: ML ≥ 4.0 or a ground motion felt on the surface within 3 km of the drilling pad </td></tr></tbody></table> <div class="mw-heading mw-heading2"><h2 id="Nuclear_explosions">Nuclear explosions</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=28" title="Edit section: Nuclear explosions">edit</a>]</div> Nuclear explosions can cause seismic activity, but according to USGS, the resulting seismic activity is less energetic than the original nuclear blast, and generally does not produce large aftershocks. Nuclear explosions may instead release the <a href="/wiki/Deformation_(engineering)" title="Deformation (engineering)">elastic strain</a> energy that was stored in the rock, strengthening the initial blast <a href="/wiki/Effects_of_nuclear_explosions" title="Effects of nuclear explosions">shockwave</a>.<a href="#cite_note-102">[102]</a> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Tired_mountain_syndrome" title="Tired mountain syndrome">Tired mountain syndrome</a></div> <div class="mw-heading mw-heading2"><h2 id="U.S._National_Research_Council_report">U.S. National Research Council report</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=29" title="Edit section: U.S. National Research Council report">edit</a>]</div> A 2013 report from the <a href="/wiki/U.S._National_Research_Council" class="mw-redirect" title="U.S. National Research Council">U.S. National Research Council</a> examined the potential for energy technologies—including shale gas recovery, carbon capture and storage, geothermal energy production, and conventional oil and gas development—to cause earthquakes.<a href="#cite_note-103">[103]</a> The report found that only a very small fraction of injection and extraction activities among the hundreds of thousands of energy development sites in the United States have induced seismicity at levels noticeable to the public. However, although scientists understand the general mechanisms that induce seismic events, they are unable to accurately predict the magnitude or occurrence of these earthquakes due to insufficient information about the natural rock systems and a lack of validated predictive models at specific energy development sites.<a href="#cite_note-dels.nas.edu-104">[104]</a> The report noted that hydraulic fracturing has a low risk for inducing earthquakes that can be felt by people, but underground injection of wastewater produced by hydraulic fracturing and other energy technologies has a higher risk of causing such earthquakes. In addition, carbon capture and storage—a technology for storing excess carbon dioxide underground—may have the potential for inducing seismic events, because significant volumes of fluids are injected underground over long periods of time.<a href="#cite_note-dels.nas.edu-104">[104]</a> <div class="mw-heading mw-heading2"><h2 id="List_of_induced_seismic_events">List of induced seismic events</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=30" title="Edit section: List of induced seismic events">edit</a>]</div> <div class="mw-heading mw-heading3"><h3 id="Table">Table</h3>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=31" title="Edit section: Table">edit</a>]</div> <table class="wikitable sortable"> <tbody><tr> <th scope="col" style="width: 120px;">Date </th> <th>Cause </th> <th>Details </th> <th scope="col" style="width: 80px;"><a href="/wiki/Seismic_magnitude_scales" title="Seismic magnitude scales">Mag.</a> </th></tr> <tr> <td>1951 </td> <td>Underground nuclear test </td> <td><a href="/wiki/Operation_Buster%E2%80%93Jangle" title="Operation Buster–Jangle">Operation Buster–Jangle</a> was a series of seven (six atmospheric, one <a href="/wiki/Explosion_crater" title="Explosion crater">cratering</a>) <a href="/wiki/Nuclear_weapon" title="Nuclear weapon">nuclear weapons</a> tests conducted by the United States in late 1951 at the <a href="/wiki/Nevada_Test_Site" title="Nevada Test Site">Nevada Test Site</a>. This was the first underground nuclear weapons test ever conducted. </td> <td>Unknown </td></tr> <tr> <td>1952 </td> <td>Wastewater injection wells </td> <td>Results of ongoing multi-year research on induced earthquakes by the <a href="/wiki/United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a> (USGS) published in 2015 suggested that most of the significant earthquakes in Oklahoma, such as the 1952 magnitude 5.7 El Reno earthquake may have been induced by deep injection of waste water by the oil industry. "Earthquake rates have recently increased markedly in multiple areas of the Central and Eastern United States (CEUS), especially since 2010, and scientific studies have linked the majority of this increased activity to wastewater injection in deep disposal wells."<a href="#cite_note-105">[105]</a> </td> <td>5.7 </td></tr> <tr> <td>1967 December 11 </td> <td>Artificial lake </td> <td>The <a href="/wiki/1967_Koynanagar_earthquake" title="1967 Koynanagar earthquake">1967 Koynanagar earthquake</a> occurred near <a href="/wiki/Koynanagar" title="Koynanagar">Koynanagar</a> town in <a href="/wiki/Maharashtra" title="Maharashtra">Maharashtra</a>, India on 11 December local time. The magnitude 6.6 shock hit with a maximum <a href="/wiki/Mercalli_intensity_scale" class="mw-redirect" title="Mercalli intensity scale">Mercalli intensity</a> of VIII (Severe). It occurred near the site of <a href="/wiki/Koyna_dam" class="mw-redirect" title="Koyna dam">Koyna dam</a>, raising questions about induced seismicity, and claimed at least 177 lives and injured over 2,200. </td> <td>6.6 </td></tr> <tr> <td>1971 November 6 </td> <td>Underground nuclear test </td> <td>Occurred on <a href="/wiki/Amchitka" title="Amchitka">Amchitka</a> island, <a href="/wiki/Alaska" title="Alaska">Alaska</a>, by the <a href="/wiki/United_States_Atomic_Energy_Commission" title="United States Atomic Energy Commission">United States Atomic Energy Commission</a>. The experiment, part of the <a href="/wiki/Operation_Grommet" title="Operation Grommet">Operation Grommet</a> nuclear test series, tested the warhead design for the <a href="/wiki/LIM-49_Spartan" title="LIM-49 Spartan">LIM-49 Spartan</a> anti-ballistic missile. With an explosive yield of almost 5-megatons <a href="/wiki/TNT_equivalent" title="TNT equivalent">TNT equivalent</a>, the test was the largest underground explosion ever detonated. The campaigning environmental organization <a href="/wiki/Greenpeace" title="Greenpeace">Greenpeace</a> grew out of efforts to oppose the test. </td> <td>7.1 <a href="/wiki/Seismic_magnitude_scales#mb" title="Seismic magnitude scales"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1038841319">mb</a> <a href="#cite_note-SIPRI-106">[106]</a> </td></tr> <tr> <td>1973 </td> <td>Geothermal power plant </td> <td>Studies have shown that injecting water into <a href="/wiki/The_Geysers" title="The Geysers">The Geysers</a> field produces earthquakes from magnitude 0.5 to 3.0, although a 4.6 occurred in 1973 and magnitude four events increased thereafter.<a href="#cite_note-107">[107]</a> </td> <td>4.6 </td></tr> <tr> <td>2006 October 9 </td> <td>Underground nuclear test </td> <td><a href="/wiki/2006_North_Korean_nuclear_test" title="2006 North Korean nuclear test">2006 North Korean nuclear test</a> </td> <td>4.3 <a href="/wiki/Seismic_magnitude_scales#mb" title="Seismic magnitude scales"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1038841319">mb</a> <a href="#cite_note-108">[108]</a> </td></tr> <tr> <td>2009 May 25 </td> <td>Underground nuclear test </td> <td><a href="/wiki/2009_North_Korean_nuclear_test" title="2009 North Korean nuclear test">2009 North Korean nuclear test</a> </td> <td>4.7 <a href="/wiki/Seismic_magnitude_scales#mb" title="Seismic magnitude scales"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1038841319">mb</a> <a href="#cite_note-109">[109]</a> </td></tr> <tr> <td>2011 November 5 </td> <td>Wastewater injection wells </td> <td><a href="/wiki/2011_Oklahoma_earthquake" title="2011 Oklahoma earthquake">2011 Oklahoma earthquake</a> </td> <td>5.8<a href="#cite_note-110">[110]</a> </td></tr> <tr> <td>2013 February 12 </td> <td>Underground nuclear test </td> <td><a href="/wiki/2013_North_Korean_nuclear_test" title="2013 North Korean nuclear test">2013 North Korean nuclear test</a> </td> <td>5.1<a href="#cite_note-111">[111]</a> </td></tr> <tr> <td>2016 January 6 </td> <td>Underground nuclear test </td> <td><a href="/wiki/January_2016_North_Korean_nuclear_test" title="January 2016 North Korean nuclear test">January 2016 North Korean nuclear test</a> </td> <td>5.1<a href="#cite_note-www.dw.com-112">[112]</a> </td></tr> <tr> <td>2016 September 9 </td> <td>Underground nuclear test </td> <td><a href="/wiki/September_2016_North_Korean_nuclear_test" title="September 2016 North Korean nuclear test">September 2016 North Korean nuclear test</a> </td> <td>5.3<a href="#cite_note-113">[113]</a> </td></tr> <tr> <td>2017 September 3 </td> <td>Underground nuclear test </td> <td><a href="/wiki/2017_North_Korean_nuclear_test" title="2017 North Korean nuclear test">2017 North Korean nuclear test</a> </td> <td>6.3<a href="#cite_note-www.dw.com-112">[112]</a> </td></tr></tbody></table> <div class="mw-heading mw-heading2"><h2 id="References">References</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=32" title="Edit section: References">edit</a>]</div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output 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Seismological Research Letters, June 10, 2015. <a rel="nofollow" class="external free" href="https://doi.org/10.1785/0220150067">https://doi.org/10.1785/0220150067</a>. </li> <li id="cite_note-101"><a href="#cite_ref-101">^</a> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFKao2019" class="citation web cs1">Kao, Hong (2019-04-09). <a rel="nofollow" class="external text" href="https://www.orogo.gov.nt.ca/sites/orogo/files/resources/induced_seismicity_workshop_-_review_of_traffic_light_protocol.pdf">"A Review of Traffic Light Protocol for Induced Seismicity and Its Effectiveness in Canada"</a> (PDF).</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=unknown&rft.btitle=A+Review+of+Traffic+Light+Protocol+for+Induced+Seismicity+and+Its+Effectiveness+in+Canada&rft.date=2019-04-09&rft.aulast=Kao&rft.aufirst=Hong&rft_id=https%3A%2F%2Fwww.orogo.gov.nt.ca%2Fsites%2Forogo%2Ffiles%2Fresources%2Finduced_seismicity_workshop_-_review_of_traffic_light_protocol.pdf&rfr_id=info%3Asid%2Fen.wikipedia.org%3AInduced+seismicity" class="Z3988"> </li> <li id="cite_note-102"><a href="#cite_ref-102">^</a> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite class="citation web cs1"><a rel="nofollow" class="external text" href="https://www.usgs.gov/faqs/can-nuclear-explosions-cause-earthquakes?qt-news_science_products=7#qt-news_science_products">"Can nuclear explosions cause earthquakes?"</a>. 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U.S. Geological Survey. Retrieved November 8, 2015. "Several lines of evidence further suggest that most of the significant earthquakes in Oklahoma during the 20th century may also have been induced by oil production activities. Deep injection of waste water, now recognized to potentially induce earthquakes, in fact began in the state in the 1930s." </li> <li id="cite_note-SIPRI-106"><a href="#cite_ref-SIPRI_106-0">^</a> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFGoldblatCox1988" class="citation book cs1">Goldblat, Jozef; Cox, David, eds. (1988). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=x9s7fSvySsMC&pg=PA80">Nuclear Weapon Tests: Prohibition or Limitation?</a>. 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Retrieved 2017-09-04.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=North+Korea+claims+success+in+fifth+nuclear+test&rft.date=2016-09-09&rft_id=https%3A%2F%2Fwww.bbc.com%2Fnews%2Fworld-asia-37314927&rfr_id=info%3Asid%2Fen.wikipedia.org%3AInduced+seismicity" class="Z3988"> </li> </ol></div></div> <div class="mw-heading mw-heading2"><h2 id="Further_reading">Further reading</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=33" title="Edit section: Further reading">edit</a>]</div> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFKisslinger1976" class="citation journal cs1">Kisslinger, C (1976). "A review of theories of mechanisms of induced seismicity". Engineering Geology. 10 (2–4): 85–98. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1976EngGe..10...85K">1976EngGe..10...85K</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2F0013-7952%2876%2990014-4">10.1016/0013-7952(76)90014-4</a>. <a href="/wiki/ISSN_(identifier)" class="mw-redirect" title="ISSN (identifier)">ISSN</a> <a rel="nofollow" class="external text" href="https://search.worldcat.org/issn/0013-7952">0013-7952</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Engineering+Geology&rft.atitle=A+review+of+theories+of+mechanisms+of+induced+seismicity&rft.volume=10&rft.issue=2%E2%80%934&rft.pages=85-98&rft.date=1976&rft.issn=0013-7952&rft_id=info%3Adoi%2F10.1016%2F0013-7952%2876%2990014-4&rft_id=info%3Abibcode%2F1976EngGe..10...85K&rft.aulast=Kisslinger&rft.aufirst=C&rfr_id=info%3Asid%2Fen.wikipedia.org%3AInduced+seismicity" class="Z3988"></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFTalwani1997" class="citation journal cs1">Talwani, P. (1997). "On the Nature of Reservoir-induced Seismicity". Pure and Applied Geophysics. 150 (3–4): 473–492. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1997PApGe.150..473T">1997PApGe.150..473T</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1007%2Fs000240050089">10.1007/s000240050089</a>. <a href="/wiki/ISSN_(identifier)" class="mw-redirect" title="ISSN (identifier)">ISSN</a> <a rel="nofollow" class="external text" href="https://search.worldcat.org/issn/0033-4553">0033-4553</a>. <a href="/wiki/S2CID_(identifier)" class="mw-redirect" title="S2CID (identifier)">S2CID</a> <a rel="nofollow" class="external text" href="https://api.semanticscholar.org/CorpusID:32397341">32397341</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Pure+and+Applied+Geophysics&rft.atitle=On+the+Nature+of+Reservoir-induced+Seismicity&rft.volume=150&rft.issue=3%E2%80%934&rft.pages=473-492&rft.date=1997&rft_id=info%3Adoi%2F10.1007%2Fs000240050089&rft_id=https%3A%2F%2Fapi.semanticscholar.org%2FCorpusID%3A32397341%23id-name%3DS2CID&rft.issn=0033-4553&rft_id=info%3Abibcode%2F1997PApGe.150..473T&rft.aulast=Talwani&rft.aufirst=P.&rfr_id=info%3Asid%2Fen.wikipedia.org%3AInduced+seismicity" class="Z3988"></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFFoulgerWilsonGluyasJulian2018" class="citation journal cs1">Foulger, G.R.; Wilson, M.P.; Gluyas, J.G.; Julian, B.R.; Davies, R.J. (2018). <a rel="nofollow" class="external text" href="https://doi.org/10.1016%2Fj.earscirev.2017.07.008">"Global review of human-induced earthquakes"</a>. Earth-Science Reviews. 178: 438–514. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2018ESRv..178..438F">2018ESRv..178..438F</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2Fj.earscirev.2017.07.008">10.1016/j.earscirev.2017.07.008</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Earth-Science+Reviews&rft.atitle=Global+review+of+human-induced+earthquakes&rft.volume=178&rft.pages=438-514&rft.date=2018&rft_id=info%3Adoi%2F10.1016%2Fj.earscirev.2017.07.008&rft_id=info%3Abibcode%2F2018ESRv..178..438F&rft.aulast=Foulger&rft.aufirst=G.R.&rft.au=Wilson%2C+M.P.&rft.au=Gluyas%2C+J.G.&rft.au=Julian%2C+B.R.&rft.au=Davies%2C+R.J.&rft_id=https%3A%2F%2Fdoi.org%2F10.1016%252Fj.earscirev.2017.07.008&rfr_id=info%3Asid%2Fen.wikipedia.org%3AInduced+seismicity" class="Z3988"></li></ul> <div class="mw-heading mw-heading2"><h2 id="External_links">External links</h2>[<a href="/w/index.php?title=Induced_seismicity&action=edit&section=34" title="Edit section: External links">edit</a>]</div> <ul><li><a rel="nofollow" class="external text" href="https://inducedearthquakes.org/">The Human-Induced Earthquake Database</a></li> <li><a rel="nofollow" class="external text" href="http://www.internationalrivers.org/en/node/3972">Map of reservoir-induced earthquakes</a> at International Rivers</li> <li><a rel="nofollow" class="external text" href="https://www.youtube.com/watch?v=v-79qW30Z2k">WEBINAR: Yes, Humans Really Are Causing Earthquakes</a> – <a href="/wiki/IRIS_Consortium" title="IRIS Consortium">IRIS Consortium</a></li> <li><a rel="nofollow" class="external text" href="https://pubs.er.usgs.gov/publication/ofr20161035">One-year seismic hazard forecast for the Central and Eastern United States from induced and natural earthquakes</a> – <a href="/wiki/United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a>, 2016 (with maps)</li> <li><a rel="nofollow" class="external text" href="https://www.usgs.gov/natural-hazards/earthquake-hazards/induced-earthquakes">Induced Earthquakes</a> – <a href="/wiki/United_States_Geological_Survey" title="United States Geological Survey">United States Geological Survey</a> website</li></ul>    </div><noscript><img src="https://login.wikimedia.org/wiki/Special:CentralAutoLogin/start?type=1x1" alt="" width="1" height="1" style="border: none; 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